A manuscript copy, with corrections and editor's notations in red, of the article published in the Philosophical Society of Washington Bulletin, volume 12, 1892.

The origin of different kinds of igneous rocks can be understood in terms of their tectonic setting, and by way of the isotope compositions of strontium, neodymium, and lead. This book explains the petrogenesis of igneous rocks as a consequence of tectonic processes resulting from interactions between asthenopheric plumes and the overlying lithospheric mantle. The relevant principles of isotope geochemistry are explained in the first chapter, making it accessible for university students as well as professionals. The relevant isotopic data is presented in diagrammatic form. The book contains more than 400 original drawings.

Hess (geological sciences, Brown U.) explores the complex process of the generation and cooling of those rocks formed by solidification from a molten state, either intrusively, below the earth's crust, or extrusively as lava. Some topics treated are: magmatic differentiation and other processes; nature of silicate melts; island-arc volcanism; continental flood basalts and rifts; lunar petrology; ocean-floor volcanism. An advanced treatment. Annotation copyrighted by Book News, Inc., Portland, OR